2007 GSA Denver Annual Meeting (28–31 October 2007)
Paper No. 30-2
Presentation Time: 1:45 PM-2:00 PM

TRILOBITE TAPHONOMY OF THE UPPERMOST DYERAN (LOWER CAMBRIAN) RUIN WASH LAGERSTÄTTE, CHIEF RANGE, NEVADA

WEBSTER, Mark, Dept. of Geophysical Sciences, University of Chicago, 5734 South Ellis Avenue, Chicago, IL 60637, mwebster@geosci.uchicago.edu, HUGHES, Nigel, Earth Sciences, Univ of California, Riverside, 1432 Geology Building, Riverside, CA 92507, and GAINES, Robert, Geology Department, Pomona College, 185 E. Sixth Street, Claremont, CA 91711

The uppermost 43 cm of Dyeran strata at Ruin Wash contain exceptionally preserved olenelloid trilobites. Detailed sedimentology and ichnology shows that the strata were deposited as a series of event beds which progressively waned then waxed in intensity up section; benthic redox conditions shifted concurrently. Biostratinomic data for 550 trilobite specimens encountered in the measured section reveal that the fauna was autochthonous, although winnowed, bioclast-rich surfaces at the base and top of the section indicate intervals of prolonged pre-burial exposure time and in situ reworking. Trilobite biostratinomy was strongly influenced by the subtle environmental shifts: the degree of disarticulation and sclerite fracturing correlate positively with event bed energy and substrate oxygenation.

Patterns of sclerite disarticulation, inversion, rotation, and fracturing were documented for almost 1300 additional specimens from the site. Two-thirds of specimens recovered were isolated cephala. Of the 389 specimens preserving cephalic plus thoracic information, only 32 (8%) represent unequivocal carcasses and 11 (3%) represent unequivocal molts: the vast majority of articulated specimens are preserved in configurations which cannot be unambiguously interpreted in terms of death posture or ecdysis-related movement. The propensity for post-ecdysial or post-mortem modification of sclerite configurations by physical or biological processes cautions against interpreting particular configurations in terms of ecdysial movements unless they consistently preserve unambiguous and functionally logical molt signatures. Recognition of such consistent ensembles demands large sample size, but provides a rigorous basis for determining ranges of molting behavior.

Extensive cephalic fracturing is found only in intervals of relatively high reworking and longer sclerite duration in the taphonomically active zone. The frequency of sclerite fracturing in unambiguous carcasses does not significantly differ from that in unambiguous molts. Sclerite damage at Ruin Wash therefore resulted primarily from physical processes, and does not provide a reliable proxy for predation or scavenging. However, predation is indicated by rare instances of healed injuries.

2007 GSA Denver Annual Meeting (28–31 October 2007)
General Information for this Meeting
Session No. 30
Paleontology II: Taphonomy and Paleoecology
Colorado Convention Center: 506
1:30 PM-5:30 PM, Sunday, 28 October 2007

Geological Society of America Abstracts with Programs, Vol. 39, No. 6, p. 88

© Copyright 2007 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.